Babine Copper - Gold Project

Copper-Gold Porphyry Belt, Central BC

The Babine Copper-Gold District is a historically active porphyry belt in Central British Columbia, home to significant Cu-Au discoveries. Hi-View’s 100%-owned Babine Project is positioned near the NAK (American Eagle) and DUKE (Amarc) deposits, in a proven mineralized corridor with extensive geophysical and geochemical support.

logistical and geological advantages

Easily accessible by road from Smithers, with nearby highway and rail connections to major ports, the Babine project benefits from strategic infrastructure and a mining-friendly jurisdiction. These logistical and geological advantages make Babine a highly prospective exploration asset in a proven copper-gold belt.

Buried Potential in Underexplored Terrain

Government sampling revealed copper anomalies over 85 ppm in till and 40 ppm in lake sediments—strong signs of buried porphyry potential. Much of the property remains unexplored due to glacial cover, offering a key discovery opportunity

Hi-View Resources holds 100% of a 609-hectare claim in B.C.’s Babine Copper-Gold district, 90 km from Smithers with highway and rail access.
The property’s favourable terrain and existing infrastructure support low-cost exploration, making Babine a strategic asset in a proven mining region.
Hi-View’s Babine claims lie 12 km southeast of American Eagle’s NAK deposit, on-trend with both NAK and Amarc’s DUKE, highlighting strong exploration potential.
Recent funding from Teck and South32 boosted American Eagle’s cash to ~$37M, backing major drilling at the nearby NAK project.

Babine Property Historical Data and Geological Context

Hi-View’s Babine claim sits at the contact of Hazelton and Takla Group rocks, a key marker for porphyry and epithermal systems. Nearby deposits like Hearne Hill, Duke, and Nak are linked to Babine Plutonic Suite intrusions, some of which are mapped just east of the claim (Nelson & Kyba, 2014).
The claims lie beneath glacial till in a deep north–northeast valley, with ice flow mapped to the south–southeast. Dispersed copper anomalies (>40 ppm in lake/stream sediments, >85 ppm in till) are found south and southeast of Nak, Duke, and Hi-View’s Babine claim—where three lake and three till samples show elevated copper.
The Search Phase II airborne magnetic survey outlines a NW structural trend from Nak, Duke, Mast, and Hautete showings that extends onto Hi-View’s Babine claim. Magnetic signals are muted over the claim, likely due to deep till and valley cover.
Search II potassium radiometric data show high values linked to Babine Plutonic Suite intrusions, with anomalies extending onto the claim. However, some radiometric data over the area appears to be missing.